基于农户视角的耕地细碎化程度评价——以湖北省“江夏区—咸安区—通山县”为例

农户是耕地最主要的经营主体,基于农户视角构建耕地细碎化程度评价指标体系更为合理。本文选取湖北省“江夏区—咸安区—通山县”作为研究区域,采用改进的TOPSIS法,利用农户问卷调查数据,对耕地细碎化程度评价进行了实证研究。结果表明：①耕地细碎化程度衡量指标的选取应基于耕地细碎化的属性特征,从农户微观视角,选取地块平均面积、地块数量、地块间的平均距离3个指标,衡量某一区域的耕地细碎化程度;②耕地细碎化在岗地平原地区与低山丘陵地区间存在显著差异,岗地平原地区的耕地细碎化程度低于低山丘陵地区;③研究区域地形地貌呈现出“北部岗地平原—南部低山丘陵”的分布特征,耕地细碎化的综合程度基本上呈现出“北部低—南部高”的分布规律;④在不同经济发展水平地区耕地细碎化存在显著差异,在岗地平原地区,经济发展水平越高的地区,耕地细碎化程度越高;而在低山丘陵地区,经济发展水平越高的地区,耕地细碎化程度越低。     

基于户籍类型比较的流动人口城市落户意愿影响机制研究

流动人口城市落户意愿是提高户籍城镇化水平,推进市民化进程的关键影响因素.从个体初始因素、中介因素和流入地城市因素3个维度,应用多水平回归模型,研究了流动人口落户意愿的影响因素,并着重比较了农业户籍流动人口和非农户籍流动人口落户意愿影响机制的差异.研究发现非农户籍流动人口比农业户籍流动人口有更强的在流入地城市落户的意愿....     

居民家庭日常出行碳排放的发生机制与调控策略——以北京市为例

根据2007年北京市居民活动日志调查数据,利用Amos7.0软件建立单效标因素的路径分析模型,试图在"社区-家庭"层面上挖掘"空间利用-出行特征-碳排放"的内在发生机理,藉此寻找城市空间组织低碳化的调控路径。研究发现:影响居民家庭日常出行碳排放的主要因素是出行距离和出行方式。社区空间利用特征对家庭出行的距离总量有显著影响,对小汽车出行比率则没有明显作用效果;私家车的购置对居民家庭出行行为的高碳化具有不可逆的作用特点;在现有设施条件、空间环境和车辆使用政策下,公共交通对私人交通出行没有替代性。研究认为,城市空间组织和调控优化应通过土地混合利用、设施供给等物质空间组织与再组织手段,形成空间行为组织和行为规划策略,引导居民降低交通发生量,优化居民交通发生的时空结构,建构低碳的城市空间结构。     

农户对农业绿色生产技术响应的影响因素 ——以青岛市为例

利用青岛市黄岛区和即墨区10个村庄共213个农户的实地调研数据,通过Logistic模型从秸秆还田、农家肥还田以及可降解农膜和绿色农药使用等方面考察农户对不同农业绿色生产技术的响应差异及影响因素。结果表明:(1)农户对农业绿色生产技术响应的影响因素确有差异。其中,施用绿色农药由农户资金情况主导,秸秆还田受种植结构和政策宣传影响较大,农家肥还田对土地规模要求较高,可降解农膜使用受种植结构影响较大。(2)户主和家庭特征对农户响应行为影响显著。(3)宣传与政策有利于促进农户采纳农业绿色生产技术,尤其是农户参与秸秆还田方面。针对结论提出了加强政策宣传与支持、开展专项教育培训、建立专项金融体系等政策建议。     

Dispersive Particle Transport: Identification of Macroscale Behavior in Heterogeneous Stratified Subsurface Flows

Dispersive mass transport processes in naturally heterogeneous geological formations (porous media) are investigated based on a particle approach to mass transport and on its numerical implementation using LPT3D, a Lagrangian Particle Tracking 3D code. We are currently using this approach for studying microscale and macroscale space–time behavior (advection, diffusion, dispersion) of tracer plumes, solutes, or miscible fluids, in 1,2,3-dimensional heterogeneous and anisotropic subsurface formations (aquifers, petroleum reservoirs). Our analyses are based on a general advection-diffusion model and numerical scheme where concentrations and fluxes are discretized in terms of particles. The advection-diffusion theory is presented in a probabilistic framework, and in particular, a numerical analysis is developed for the case of advective transport and rotational flows (numerical stability of the explicit Euler scheme). The remainder of the paper is devoted to the behavior of concentration, mass flux density, and statistical moments of the transported tracer plume in the case of heterogeneous steady flow fields, where macroscale dispersion occurs due to geologic heterogeneity and stratification. We focus on the case of perfectly stratified or multilayered media, obtained by generating many horizontal layers with a purely random transverse distribution of permeability and horizontal velocity. In this case, we calculate explicitly the exact mass concentration field C(x, t), mass flux density field f(x, t), and moments. This includes spatial moments and dispersion variance ² _x (t) on a finite domain L, and temporal moments on a finite time scale T, e.g., the mass variance of arrival times ² _T (x). The moments are related to flux concentrations in a way that takes explicitly into account finite space–time scales of analysis (time-dependent tracer mass; spatially variable flow through mass). The multilayered model problem is then used in numerical experiments for testing different ways of recovering information on tracer plume migration, dispersion, concentration and flux fields. Our analyses rely on a probabilistic interpretation that emerges naturally from the particle approach; it is based on spatial moments (particle positions), temporal moments (mass weighted arrival times), and probability densities (both concentrations and fluxes). Finally, as an alternative to direct estimations of the flux and concentration fields, we formulate and study the Moment Inverse Problem. Solving the MIP yields an indirect method for estimating the space–time distribution of flux concentrations based on observed or estimated moments of the plume. The moments may be estimated from field measurements, or numerically computed by particle tracking as we do here.     

On the instability of internal gravity waves propagating at small but finite angles to the vertical

The question of the instability of internal gravity waves (IGWs) propagating at small angles to the vertical is re-visited. The case of an IGW of finite-amplitude propagating at a very small but finite angle to the vertical is considered. This angle serves as a small parameter in the problem, and the instability of such an IGW is investigated by using the Fourier method and the Sivashinsky integral relations. The analysis undertaken confirms the existence of short-wave instability for small IGW amplitudes and for an arbitrarily small value of their propagation angle to the vertical. For small viscosity and thermal conductivity of the fluid medium, the growth rate of the most unstable mode is proportional to the square of the amplitude of the IGW. The results obtained may be of interest for interpreting the results of observations and confirming the existence of turbulence in the middle atmosphere.     

Turbulent Statistics of Neutrally Stratified Flow Within and Above a Sparse Forest from Large-Eddy Simulation and Field Observations

Turbulent statistics of neutrally stratified shear-driven flow within and above a sparse forest canopy are presented from a large-eddy simulation (LES) and compared with those from observations within and above a deciduous forest with similar height and foliage density. First- and second-order moments from the LES agree with observations quite well. Third-order moments from the LES have the same sign and similar vertical patterns as those from the observations, but the LES yields smaller magnitudes of such higher-order moments. Turbulent spectra and cospectra from the LES agree well with observations above the forest. However, at the highest frequencies, the LES spectra have steeper slopes than observations. Quadrant and conditional analyses of the LES resolved-scale flow fields also agree with observations. For example, both LES and observation find that sweeps are more important than ejections for the transport of momentum within the forest, while inward and outward interaction contributions are both small, except near the forest floor. The intermittency of the transport of momentum and scalar increases with depth into the forest. Finally, ramp structures in the time series of a passive scalar at multiple levels within and above the forest show similar features to those measured from field towers. Two-dimensional (height-time cross-section) contours of the passive scalar and wind vectors show sweeps and ejections, and the characteristics of the static pressure perturbation near the ground resemble those deduced from field tower-based measurements. In spite of the limited grid resolution (2 m × 2 m × 2 m) and domain size (192 m × 192 m × 60 m) used in this LES, we demonstrate that the LES is capable of resolving the most important characteristics of the turbulent flow within and above a forest canopy.     

层状岩质边坡破坏模式及稳定性的数值分析

运用FLAC3D模拟层状岩质边坡的破坏模式,并采用强度折减法分析结构面倾角与稳定性之间的关系。结果表明:①水平层状边坡坡顶变形破坏早于坡面和坡脚,形成拉破坏区。当结构面倾角较小时,顺倾向层状边坡主要发生滑移破坏;当结构面倾角较大时,发生弯折-溃曲破坏。直立层状边坡主要发生弯曲-板间拉裂-塌落破坏。逆倾向层状边坡的破坏形式为对于小倾角为滑移破坏,对于陡倾角为倾倒破坏。②对于顺倾向边坡,整体安全系数随结构面倾角先减小后增大,呈现两头高、中间低的形态,在倾角为30°时安全系数最小;对于逆倾向边坡,曲线呈现增大-减小-增大的态势,并且大部分高于顺倾向边坡曲线,符合实际情况。③所采用的低强度弹塑性单元能够比较真实地模拟软弱结构面的变形。     

Thermohaline convection in flowing groundwater

Geothermal activity creates destabilising temperature gradients which are significant in some aquifers. Usually, in such aquifers stabilising salinity gradients also exist. The combination of temperature and salinity distribution in the aquifer may induce various types of hydrodynamic instabilities which were identified in a previous article. The present article concerns the effect of anisotropic characteristics of the hydrodynamic dispersion on the growth of instabilities in the aquifer. Three different mechanisms may lead to instability of the flow field: (a) buoyancy forces may induce convection currents; if the difference between the convection velocity of salt, due to the hydraulic gradients, and that of heat is negligible, then this mechanism is generally most effective in planes parallel to the hydraulic velocity of the fluid (velocity due to the hydraulic gradient); (b) the difference between heat and salt effective diffusivities may lead to overstability; this mechanism is most effective in planes perpendicular to the hydraulic velocity; (c) the difference between the convection velocity of salt and that of heat may induce oscillations which are most effective in planes parallel to the hydraulic velocity. The growth of instabilities in an aquifer of unlimited length is different from their growth in an aquifer of limited length. In the latter thermohaline convection develops in planes perpendicular to the hydraulic velocity, whereas in the former it develops in planes forming an angle θ with the hydraulic gradient. The development of convection cells in the flow field is identified by numerical experiments. These experiments identify the convection cell length and the angle formed between the thermohaline convection plane and the hydraulic gradient.     

Petrogenesis of Mafic Inclusions in Rhyolitic Lavas from Narugo Volcano, Northeastern Japan

Mafic inclusions present in the rhyolitic lavas of Narugo volcano,Japan, are vesiculated andesites with diktytaxitic texturesmainly composed of quenched acicular plagioclase, pyroxenes,and interstitial glass. When the mafic magma was incorporatedinto the silica-rich host magma, the cores of pyroxenes andplagioclase began to crystallize (>1000°C) in a boundarylayer between the mafic and felsic magmas. Phenocryst rim compositionsand interstitial glass compositions (average 78 wt % SiO₂) inthe mafic inclusions are the same as those of the phenocrystsand groundmass glass in the host rhyolite. This suggests thatthe host felsic melt infiltrated into the incompletely solidifiedmafic inclusion, and that the interstitial melt compositionin the inclusions became close to that of the host melt (c.850°C). Infiltration was enhanced by the vesiculation ofthe mafic magma. Finally, hybridized and density-reduced portionsof the mafic magma floated up from the boundary layer into thehost rhyolite. We conclude that the ascent of mafic magma triggeredthe eruption of the host rhyolitic magma. KEY WORDS: mafic inclusion; stratified magma chamber; magma mixing; mingling; Narugo volcano; Japan